Injection in the very small Vale geothermal aquifer does not appear to be beneficial. Water levels and temperature in the upflow zone are dropping. Natural surface spring discharge has ceased. Temperatures in the outflow zone have decreased and well shut-in pressure occurred where before injection there was no pressure. New springs have surfaced near injection wells. The cause seems to be that injection is across a hydrogeologic boundary from production. Injection on the same side of the boundary does not appear possible